Sea ice variability is a key indicator of climate variability and change in the polar regions. The primary parameters that define the state of sea ice include: concentration, area and extent, ice type, motion, deformation, age, thickness, and volume. The presence of sea ice strongly modifies surface waves and air-sea exchanges of heat, momentum, moisture and gases. Sea ice has a significant impact on the Earth’s albedo and hence changes in Sea Ice impact the global energy budget. The properties of many water masses of the global ocean and strongly influenced determined freezing and melting processes in sea ice regions.
Sea Ice Concentration
ECV Products and Requirements
These products and requirements reflect the Implementation Plan 2022 (GCOS-244).
The requirements are found in the complete 2022 ECVs Requirements document as well: ECV Sea Ice.
Products | | Sea Ice Concentration | | | Sea Ice Thickness | | | Sea Ice Drift | | | Sea Ice Age |
| (*) | Unit | Values | | Unit | Values | | Unit | Values | | Unit | Values |
Horizontal Resolution | G | km | 1 | | km | 1 | | km | 1 | | km | 1 |
B | 5 (reg. analysis), 25 (trend analysis) | | 25 | | 5-25 | | 5-25 |
T | 50 | | 50 | | 50 | | 50 |
Vertical Resolution | G | | | | | - | | | - | | | - |
B | | | - | | - | | - |
T | | | - | | - | | - |
Temporal Resolution | G | d | <1 | | d | 1 | | d | <1 | | d | <1 |
B | 1 (reanalysis), 7 daily monitoring | | 7-30 | | 1-7 | | 1-7 |
T | 30 | | 30 | | 30 | | 30 |
Timeliness | G | d | 1-2 | | d | 1 | | d | 1-2 | | d | 1-2 |
B | 7 | | 7 | | 7 | | 7 |
T | 30 | | 30 | | 30 | | 30 |
Required Measurement Uncertainty (2-sigma) | G | % SIC | 5 | | m | 0.05 | | km d-1 | 0.25 | | d | 7 |
B | | | 0.1 | | 3 | | 182 |
T | 10 | | 0.25 | | 10 | | >365 |
Stability | G | %/decade | 5 | | m/decade | | | m/decade | | | d | |
B | | | | | | | |
T | | | | | | | |
Products | | Sea Ice Temperature | | | Sea Ice Surface Albedo | | | Snow Depth on Sea Ice |
| (*) | Unit | Values | | Unit | Values | | Unit | Values |
Horizontal Resolution | G | km | 1 | | km | 1 | | km | 1 |
B | 5-10 | | 5-10 | | 25 |
T | 50 | | 50 | | 50 |
Vertical Resolution | G | | - | | | - | | | |
B | - | | - | | |
T | - | | - | | |
Temporal Resolution | G | d | 3 h | | d | 3 h | | d | 1 |
B | 1 | | 1 | | 7-30 |
T | 7 | | 7 | | 30 |
Timeliness | G | d | 1-2 | | d | 1-2 | | d | 1-2 |
B | 7 | | 7 | | 7 |
T | 30 | | 30 | | 30 |
Required Measurement Uncertainty (2-sigma) | G | K | 1 | | | 1 | | m | 0.01 |
B | 3 | | 3 | | 0.05 |
T | 6 | | 6 | | 0.1 |
Stability | G | K/decade | 0.1 | | | 0.01 | | m/decade | |
B | 0.2 | | 0.05 | | |
T | 0.3 | | 0.1 | | |
(*) Goal (G): an ideal requirement above which further improvements are not necessary. Breakthrough (B): an intermediate level between threshold and goal which, if achieved, would result in a significant improvement for the targeted application. The breakthrough value may also indicate the level at which specified uses within climate monitoring become possible. It may be appropriate to have different breakthrough values for different uses. Threshold (T): the minimum requirement to be met to ensure that data are useful